Physics Education Department - UNS 1 From the Last Time Today: Radioactivity Nucleus: –System of protons and neutrons bound by the strong force Proton.

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Presentation transcript:

Physics Education Department - UNS 1 From the Last Time Today: Radioactivity Nucleus: –System of protons and neutrons bound by the strong force Proton number determines the element. Different isotopes have different # neutrons. –Stable isotopes generally have similar number of protons and neutrons. –Too many of either results in a higher energy state: either nuclear energy state or coulomb energy state Some isotopes unstable, radioactively decay

Physics Education Department - UNS 2 protons neutrons Populating nucleon states Quantum states for nucleons in the nucleus –Similar to the hydrogen atom: one electron in each quantum state. –Two states at each energy (spin up & spin down) Helium This is 4 He, with 2 neutrons and 2 protons in the nucleus In the lowest possible energy state

Physics Education Department - UNS 3 Other(less stable) helium isotopes protons neutrons protons neutrons Too few neutrons, -> protons too close together. High Coulomb repulsion energy Too many neutrons, requires higher energy states.

Physics Education Department - UNS 4 Radioactivity Most stable nuclei have about same number of protons as neutrons. If the energy gets too high, nucleus will spontaneously try to change to lower energy configuration. These nuclear are unstable, and are said to decay. They are called radioactive nuclei.

Physics Education Department - UNS 5 Stability of nuclei Dots are naturally occurring isotopes. Larger region is isotopes created in the laboratory. Observed nuclei have ~ N=Z Slightly fewer protons because they cost Coulomb repulsion energy.

Physics Education Department - UNS 6 Radioactive nuclei ~ equal # neutrons and protons

Physics Education Department - UNS 7 Radioactive decay Decay usually involves emitting some particle from the nucleus. Generically refer to this as radiation. Not necessarily electromagnetic radiation, but in some cases it can be. The radiation often has enough energy to strip electrons from atoms, or to sometimes break apart chemical bonds in living cells.

Physics Education Department - UNS 8 Discovery of radioactivity Accidental discovery in 1896 Henri Becquerel was trying to investigate x-rays (discovered in 1895 by Roentgen). Exposed uranium compound to sunlight, then placed it on photographic plates Believed uranium absorbed sun’s energy and then emitted it as x-rays. On the 26th-27th February, experiment "failed" because it was overcast in Paris. Becquerel developed plates anyway, finding strong images, Proved uranium emitted radiation without an external source of energy.

Physics Education Department - UNS 9 Detecting radiation A Geiger counter Radiation ionizes (removes electrons) atoms in the counter Leaves negative electrons and positive ions. Ions attracted to anode/cathode, current flow is measured

Physics Education Department - UNS 10 A random process The particle emission is a random process –It has some probability of occurring. For every second of time, there is a probability that the nucleus will decay by emitting a particle. If we wait long enough, all the radioactive atoms will have decayed.

Physics Education Department - UNS 11 Radioactive half-life Example of random decay. Start with 8,000 identical radioactive nuclei Suppose probability of decaying in one second is 50%. t=0t=1 sec t=2 sec t=3 sec The half-life is one second Every second, half the atoms decay Undecayed nuclei

Physics Education Department - UNS 12 Radioactive decay question A piece of radioactive material is initially observed to have 1,000 decays/sec. Three hours later, you measure 125 decays / second. The half-life is A.1/2 hour B.1 hour C.3 hours D.8 hours In each half-life, the number of radioactive nuclei, and hence the number of decays / second, drops by a factor of two. After 1 half life, the decays/sec drop to 500. After 2 half lives it is 250 decays/sec After 3 half lives there are 125 decays/sec.

Physics Education Department - UNS 13 Another example 232 Th has a half-life of 14 billion years Sample initially contains 1 million 232 Th atoms Every 14 billion years, the number of 232 Th nuclei goes down by a factor of two.

Physics Education Department - UNS 14 Nuclear half-lives Number of neutrons Number of protons (Z)

Physics Education Department - UNS 15 Different types of radioactivity Unstable nuclei decay by emitting some form of energy, Three different types of decay observed: Alpha decay Beta decay Gamma decay (First three letters of Greek alphabet). Ernest Rutherford (1899): "These experiments show that the uranium radiation is complex and that there are present at least two distinct types of radiation - one that is very readily absorbed, which will be termed for convenience the alpha-radiation, and the other of more penetrative character which will be termed the beta-radiation."

Physics Education Department - UNS 16 Penetrating power of radiation Alpha radiation very weak Beta radiation penetrates farther Gamma radiation hardest to stop

Physics Education Department - UNS 17 Is the radiation charged? Alpha radiation positively charged Beta radiation negatively charged Gamma radiation uncharged

Physics Education Department - UNS 18 Alpha radiation Alpha radiation now known to be a helium nucleus (2 protons, 2 neutrons) Piece of atom (alpha particle) is broken from heavy nucleus and ejected

Physics Education Department - UNS 19 A new element When a nucleus emits an alpha-particle, it loses two neutrons and two protons. It becomes a different element (the number of protons in the nucleus has changed). Example: 92 protons 146 neutrons 90 protons 144 neutrons 2 protons 2 neutrons Alpha particle Thorium is the element with 90 electrons (and hence 90 protons in the nucleus)

Physics Education Department - UNS 20 Why? Why does a piece come out of the atom? –All nucleons (neutrons & protons) attracted by short-range strong force –Protons forced apart by long-range Coulomb force. –Smaller nuclei will be more stable Why is the ejected piece an alpha-particle, and not something else? –Helium nucleus is much more stable than other light nuclei –Smaller Thorium nucleus more stable as well –Overall energy state is less

Physics Education Department - UNS 21 Decay question Radium was isolated by Marie Curie in It has a half-life of 1,600 years and decays by alpha-emission. The resulting element is A. Polonium (84 electrons) B. Thorium (90 electrons) C. Radon (86 electrons)

Physics Education Department - UNS 22 Decay chain originates at 238 U Number of neutrons Number of protons  decay

Physics Education Department - UNS 23 A use for alpha-decay Smoke detectors contain radioactive americium-241 (half-life 432 yrs) 241 Am decays by alpha emission. Alpha particles from the americium collide with oxygen and nitrogen particles in the air creating charged ions. An electrical current is applied across the chamber in order to collect these ions (just like geiger counter!) When smoke is in chamber, smoke absorbs alpha particles. Current decreases, detected by electronics

Physics Education Department - UNS 24 Decay sequence of 238 U Number of neutrons Number of protons  decay But what are these?

Physics Education Department - UNS 25 A different kind of decay Number of neutrons Number of protons Number of neutrons decreases by one Number of protons increases by one How could this happen?

Physics Education Department - UNS 26 Beta decay Beta radiation… –Now know to be an electron. –Radioactive nucleus emits an electron How can this be? –There are no electrons in the nucleus! –Has only neutrons and protons. Particles are not forever! –Charge is forever, energy+mass is forever –But particles can appear and disappear or be changed

Physics Education Department - UNS 27 Beta decay Nucleus emits an electron (negative charge) Must be balanced by a positive charge appearing in the nucleus. This occurs as a neutron changing into a proton

Physics Education Department - UNS 28 How can this be? Nucleons have an internal structure. Made up of different types of quarks. In this sense, neutrons and protons not so different.

Physics Education Department - UNS 29 Quark structure of nucleons Proton = up+up+down Charge = 2/3+2/3-1/3 = +1 Neutron = up+down+down charge = 2/3-1/3-1/3 = 0

Physics Education Department - UNS 30 Neutron decay Can be clearer to visualize this diagramatically. One of the down quarks changed to an up quark. We identify this new combination of quarks as a proton. A new process unlike any other we’ve seen: The Weak Force

Physics Education Department - UNS 31 Example of beta decay 14 C (radioactive form of carbon) decays by beta decay (electron emission). Carbon has 6 electrons, so six protons. 14 C has (14-6)=8 neutrons. Now have a new element (one more proton) Element with 7 protons in nucleus is Nitrogen Beta decay number of nucleons stays fixed, but one of the neutrons changes into a proton one additional proton -> different element!

Physics Education Department - UNS 32 Radioactive carbon 14 C naturally present in the atmosphere as a result of transmutation of 14 N. Cosmic ray proton shatters nucleus of atmospheric gas atom. This produces neutrons. Neutron knocks proton out of 14 N nucleus. 14 N becomes 14 C after losing neutron

Physics Education Department - UNS 33 Natural atmospheric abundance 14 C is produced at a particular rate from transmutation of 14 N in upper atmosphere. 14 C is radioactive with half-life of 5,730 yrs –Decays at rate set by half-life Balance of these results in an equilibrium ratio in the atmosphere One radioactive 14 C atom for every ~ non-radiocative 12 C atom.

Physics Education Department - UNS C to 12 C ratio 14 C has a half-life of ~6,000 years, continually decaying back into 14 N. Steady-state achieved in atmosphere, with 14 C: 12 C ratio ~ 1:1 trillion (1 part in ) As long as biological material alive, atmospheric carbon mix ingested (as CO 2 ), ratio stays fixed. After death, no exchange with atmosphere. Ratio starts to change as 14 C decays

Physics Education Department - UNS 35 Carbon-dating question The 14 C: 12 C ratio in a fossil bone is found to be 1/8 that of the ratio in the bone of a living animal. The half-life of 14 C is 5,730 years. What is the approximate age of the fossil? A.7,640 years B.17,200 years C.22,900 years D.45,800 years Since the ratio has been reduced by a factor of 8, three half-lives have passed. 3 x 5,730 years = 17,190 years

Physics Education Department - UNS 36 Other carbon decays Lightest isotopes of carbon are observed to emit a particle like an electron, but has a positive charge! This is the antiparticle of the electron. Called the positron.

Physics Education Department - UNS 37 What is going on? 14 C has more neutrons than the most stable form 12 C. –So it decays by electron emission, changing neutron into a proton. Other isotopes of carbon have fewer neutrons –Decays by emitting positron, changing proton into neutron.

Physics Education Department - UNS 38 Gamma decay So far –Alpha decay: alpha particle emitted from nucleus –Beta decay: electron or positron emitted Both can leave the nucleus in excited state –Just like a hydrogen atom can be in an excited state –Hydrogen emits photon as it drops to lower state. Nucleus also emits photon as it drops to ground state This is gamma radiation But energies much larger, so extremely high energy photons.

Physics Education Department - UNS 39 Turning lead into gold The transmutation of platinum into gold accomplished by a sequence of two nuclear reactions first: 198 Pt + neutron --> 199 Pt second: 199 Pt --> 199 Au + subatomic particle Radioactive decay changes one element into another by changing the number of protons in a nucleus. This can also be done artificially by neutron bombardment.